texas commission on environmental quality - TCEQ e-Services
texas commission on environmental quality - TCEQ e-Services
texas commission on environmental quality - TCEQ e-Services
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Secti<strong>on</strong> 2.5.2 and Appendix 2.6.1.<br />
3. Comment: The applicati<strong>on</strong> in Volume 1, p. 2-41, describes “minor volcanism in Trans-<br />
Pecos Texas and northeastern New Mexico” as occurring “between about 27 and 31 milli<strong>on</strong><br />
years ago” and references Henry and Price, 1985. A reference check indicates that this reference<br />
does not characterize the volcanism as minor (especially as it c<strong>on</strong>tinues well into Mexico), says<br />
little or nothing about northeastern New Mexico, and states that “most of the activity, including<br />
all caldera formati<strong>on</strong>, was between 38 and 28 m.y.a.”<br />
Requested Acti<strong>on</strong>: The Applicant did not revise the text, as stated. Instead, the reference<br />
was completely omitted. Please include the reference, using the correct dates.<br />
4. Comment: We were unable to find Table 1, “Fault Source Parameters for the WCS<br />
Analysis,” in Volume 2B, Appendix 2.5.2.<br />
Requested Acti<strong>on</strong>: Please provide the table, or direct us to where it can be found in the<br />
applicati<strong>on</strong>.<br />
5. Comment: Answered in TNOD1 resp<strong>on</strong>se.<br />
6. Comment: Answered in TNOD1 resp<strong>on</strong>se.<br />
7. Comment: Answered in TNOD1 resp<strong>on</strong>se.<br />
8. Comment: Answered in TNOD1 resp<strong>on</strong>se.<br />
9. Comment: Answered in TNOD1 resp<strong>on</strong>se.<br />
10. Comment: It is not clear from Volume 3, Figure 6.4-11 how deep the main reverse fault<br />
propagates into the Dockum.<br />
Requested Acti<strong>on</strong>: Applicati<strong>on</strong> materials have provided some evidence of distributed shear<br />
upward with loss of displacement <strong>on</strong> the main fault planes. Please explain the evidence<br />
that there is also loss of displacement <strong>on</strong> the main fault planes downward, and how it has<br />
been dem<strong>on</strong>strated that displacement does not, in fact, increase downward.<br />
11. Comment: From Figure 6.4-11 in Volume 3, it appears that the sandst<strong>on</strong>e cut by the main<br />
fault may intersect with the southern sidewall of the FWF.<br />
Requested Acti<strong>on</strong>: The Applicant’s resp<strong>on</strong>se states that this sandst<strong>on</strong>e is present in B<br />
32/32A and B-60. Figure 6.4-11 in Volume 3 has the top of the sandst<strong>on</strong>e at approximately<br />
32 feet below the top of Dockum and dipping northward at the north end of the figure. The<br />
Attachment 2<br />
Sec<strong>on</strong>d Technical Notice of Deficiency<br />
1/30/2006 Page 25 of 51